Periphery deformations and tunneling at correlated quantum-Hall edges

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Surface ettlements due to deformation of a tunnel in an elastic half plane

Surface  ettlements due to deformation of a tunnel in an elastic half plane
Verruijt, A. & Booker, J. R. (1996). GeÂotechnique 46, No. 4, 753±756
TECHNICAL NOTE
Surface settlements due to deformation of a tunnel in an elastic half plane
Because of the symmetry of these two solutions, the shear stress ózx and the vertical displacement uz will be zero at the surface z 0. The normal
stresses ózz induced by the two singular solutions are equal, and add up to
of the solution and their images are


ux

ÀåR2 äR2
rxx21(x2

x
r22 À kz21) r41
ห้องสมุดไป่ตู้

x(x2
À r42
kz22)
(1)
uz

ÀåR2 äR2
rzz1211(kxrz2222 À r41
z21)

z2(kx2 À r42
thus will be small compared to the present one if
the radius R of the tunnel is small enough.
Taken together, the expressions for the displace-

中国地质大学(北京)考博专业英复习材料

中国地质大学(北京)考博专业英复习材料

晶) is said to have a porphyritic texture(斑状结构). The classification of fine-grained rocks, then, is based on the proportion of minerals which form phenocrysts and these phenocrysts (斑晶)reflect the general composition of the remainder(残留) of the rock. The fine-grained portion of a porphyritic(斑岩) rock is generally referred to as the groundmass(基质) of the phenocrysts. The terms "porphyritic" and "phenocrysts" are not restricted to fine-grained rocks but may also apply to coarse-grained rocks which contain a few crystals distinctly larger than the remainder. The term obsidian(黑曜岩) refers to a glassy rock of rhyolitic(流纹岩) composition. In general, fine-grained rocks consisting of small crystals cannot readily be distinguished from③ glassy rocks in which no crystalline material is present at all. The obsidians, however, are generally easily recognized by their black and highly glossy appearanceass of the same composition as obsidian. Apparently the difference between the modes of formation of obsidian and pumice is that in pumice the entrapped water vapors have been able to escape by a frothing(起泡) process which leaves a network of interconnected pore(气孔) spaces, thus giving the rock a highly porous (多孔的)and open appearance(外观较为松散). ④ Pegmatite(结晶花岗岩) is a rock which is texturally(构造上地) the exact opposite of obsidian. ⑤ Pegmatites are generally formed as dikes associated with major bodies of granite (花岗岩) . They are characterized by extremely large individual crystals (单个晶体) ; in some pegmatites crystals up to several tens of feet in length(宽达几十英尺)have been identified, but the average size is measured in inches (英寸) . Most mineralogical museums contain a large number of spectacular(壮观的) crystals from pegmatites. Peridotite(橄榄岩) is a rock consisting primarily of olivine, though some varieties contain pyroxene(辉石) in addition. It occurs only as coarse-grained intrusives(侵入), and no extrusive(喷出的) rocks of equivalent chemical composition have ever been found. Tuff (凝灰岩)is a rock which is igneous in one sense (在某种意义上) and sedimentary in another⑥. A tuff is a rock formed from pyroclastic (火成碎 屑的)material which has been blown out of a volcano and accumulated on the ground as individual fragments called ash. Two terms(igneous and sedimentary) are useful to refer solely to the composition of igneous rocks regardless of their textures. The term silicic (硅质 的)signifies an abundance of silica-rich(富硅) and light-colored minerals(浅 色矿物), such as quartz, potassium feldspar(钾长石), and sodic plagioclase (钠长石) . The term basic (基性) signifies (意味着) an abundance of dark colored minerals relatively low in silica and high in calcium, iron, and

roctest telemac双轴倾斜仪系统说明书

roctest telemac双轴倾斜仪系统说明书

DIGITAL INCLINOMETER SYSTEMModel DIS-500APPLICATIONSThe DIS-500 inclinometer probe is used to locate thedepth and measure the lateral displacement anddeformation of soil, rock and retaining structures todetermine:• Stability of natural and man-made slopes• Stability of embankments and dams• Deformation of sheet piles and diaphragm walls• Ground deformation due to tunneling• Movement of bridge piers and abutments• Defl ection of laterally loaded pilesDESCRIPTIONThe Roctest Telemac biaxial inclinometer system com-prises a probe, cable reel and PDA. The probe is fi tted with guide wheels and contains two MEMS accelero-meters measuring in A and B planes. It is connected by a graduated cable to the cable reel. The “read” button on the PDA or a remote handheld activator allow for the saving of readings from the accelerometers. These are transmitted cable-free to the PDA and saved via Bluetooth transmission.Completely redesigned to incorporate modern techno-logy and materials, the DIS-500 Digital Bluetooth Incli-n ometer enables highly accurate reading of lateral de-fl ections. The Kevlar reinforced cable provides strength while ena b ling signifi cant weight reductions. Wireless connection between the instrument and the PDA makes taking readings fast, simple and has none of the issues associated with fi eld connections. Strong but extremely light the instrument can be easily carried and used by one person. The modern answer to Inclino-meter data gathering.FEATURES• Digital from probe to PDA overcomingcable electrical resistance and noise issues.• No fi eld connections required, avoids water ingress and connection failures.• Solid state electronics ensure long, trouble free use in a site environment• Light, easily portable by one person• Metal Marker/Cable Gate system ensures a high degree of accuracy and repeatability• PDA allows easy interface with most offi ce systems and applications.• Enhanced PDA Sofware provides a rangeof presentations with built in “current borehole” back up facility.Products and specifications are subject to change without notice. E5DIS500-061212© Roctest Limited, 2006.SPECIFICATIONSPROBECalibrated range ±30º (standard) or ±90º (optional)Sensor accuracy ±0.02% F .S.System accuracy* ±2 mm (0.07") over 25 m (82.02')Resolution 0.01 mm (0.00039")Repeatability ±0.008% F .S.Operating −20ºC to +50ºC temperature Wheel base 500 mm (metric) or24 inches (imperial)Watertightness Up to 400 m of H 2O Probe diameter 28 mm (1 1/8")Inclinometer casing From 48 mm (1.89")internal diameters to 83 mm (3.27")CABLELength 30, 50, 75, 100, 125, 150,175, 200 m (100, 200, 300 ft)Cable marker Hard anodized colour codedType Kevlar re-enforced Polyurethanecoated 4 core cableWeight Approx 42 g per meter(0.028 lbs/ft)*Derived empirically from surveys that include systematic andrandom errors introduced by casing, probe and operator.CABLE REELDimensions 483 × 383 × 315 mm Battery life 12 hrs continuous useWeight8.5 kg (30 m), 9.5 kg (50 m), (complete with probe)11.5 kg (100 m)PDA (DIGITAL READOUT)Display QVGA, VGA TFT Color 16-bit,touch-sensitive, 3.5-in Memory card capacity 64 MB Initial database size 200 KBProgram footprint 128 KB Internal batteries 2.2 Ah rechargeable,removable, lithium-ion, with external batterycharger inputBattery life 8 to 12 hours(with or without backlight on)Interfacing USB jumper cableand memory cardOperating temperature 0°C to +40°CREMOTE HANDHELD ACTIVATOR Dimensions 65 × 35 × 15 mmWeight 26 g Battery 1 × GP23AORDERING INFORMATIONBasic inclinometer system includes probe, cable, cable reel, PDA, PDA batteries, battery chargers, USB jum-per cable, PDA carrying case, dry pack, In-Port PDA based software, remote handheld activator, and ca-ble gate for 85-mm casing (also fi ts 70-mm casing).Please specify:• Type of probe (metric or imperial)• Length of cable • AccessoriesACCESSORIESPART NUMBERDESCRIPTION99-099G11 Battery charger for inclinometer reel (Replacement)99-099G10 PDA cradle 99-099G09 High capacity battery pack for extendedPDA battery life (Replacement)99-099G08 Key fob (remote handheld activator)(Replacement)99-099G07 Dry pack for PDA (Replacement)99-099G05Cable gate for 70-mm casing99-099G06 Cable gate for 85-mm casing (Replacement)99-099G04 PDA alone with in-port software loaded (Replacement)99-099G01 In-site software for data managementwith 1 licence99-099G02 In-site software for data managementwith 2 or 3 licences99-099G03 In-site software for data managementwith 4 to 10 licences99-SOFTGTILTW GTILT Software for data management 99-SOFTGTILTPWGTILT+ Software for data management。

地质专业英语翻译段落 (学习版)

地质专业英语翻译段落 (学习版)

Petroleum occurs widely in the earth as gas,liquid,semisolid,or solid,or in more than one of these states at a single place.Chemically any petroleum is an extremely complex mixture of hydrocarbon compounds,with minor amounts of nitrogen ,oxygen,and sulfur as impurities.Liquid petroleum ,which is called crude oil to distinguish it from refined oil,is the most important commercially .It consists chiefly of the liquid hydrocarbons ,with varying amounts of dissolved gases,bitumens,and impurities.石油,以气态、液态、半固态或固态、或在某一个地方以一种以上形态广泛存在于地球中。

从化学上讲,任何石油都是由烃化合物组成的极其复杂的混合物,并含有少量作为杂质的氮、氧及硫。

液态的石油,为区别于炼制油,成为原油,在商业上是重要的。

它主要由液态烃类组成,并含有不同数量的溶解气、沥青和杂质。

The origin and distribution of a reservoir rock are controlled primarily by the processes by which the sand was deposited. Scientists concerned with the origin of sedimentary rocks are fortunate because they can observe the conditions and processes by which sediments accumulate today and use their observations to interpret the origin of ancient sediment. By using the areas of modern environments of deposition as natural laboratories, scientists seek to improve the quality of their work. A massive effort has been underway for the past 30 years by industry, government and university scientists throughout the world to investigate modern environments of deposition and to interpret the results of the processes in Holocene sequences. Concepts have evolved from these studies that have revolutionized scientific thought about the sedimentary rocks.储集岩的成因和分布基本受砂沉积时的一些作用控制。

具有温度梯度与垂直通流的多孔介质中的对流(英文)

具有温度梯度与垂直通流的多孔介质中的对流(英文)

S0017-9310(97)00103-8
TECHNICAL NOTES
Convection in a porous medium with inclined temperature gradient and vertical throughflow
D. A. N I E L D Department of Engineering Science, University of Auckland, Private Bag 92109, Auckland, New Zealand
where am = km/(pcp)f and A = (pCm)/(pcp) f. The non-dimensional parameters which arise are the throughΒιβλιοθήκη low P6clet number
Q~ = w v H / %
(6)
the vertical Rayleigh number
where the square brackets denote 'integer part of'. The standard procedure [2, 3] leads to the eigenvalue equation in the form det(A0) = 0 where, for m, n = 1, 2 A2., 12,, ~1 = (Dw~Dw.+ct2w.,w.) A~., I.~.~,--~2(w.,O.,) 72.,.2. 1 = (DTO~w,,-i~ 2kRhO.,Dw,~) A 2.,.2,, - (DO.,DO. + (c~2 (26)
L=~- -g+Q/_
Qve Rh + Rh 2 2Q~ sinh (Q~/2) [exp(Q~z) -cosh(Qv/2)]. (17)

固体电解质渗流 英语

固体电解质渗流 英语

固体电解质渗流英语Solid Electrolyte Percolation.Solid electrolyte percolation is a complex process that occurs within solid electrolytes, which are materials that allow the movement of ions or electrons without the needfor a liquid medium. This movement is crucial in various electrochemical devices such as batteries and fuel cells. Solid electrolyte percolation is the formation of conductive pathways within the solid electrolyte, enabling efficient ion or electron transport.The formation of these conductive pathways is often influenced by the microstructure of the solid electrolyte. In solid electrolytes, the movement of ions or electrons is typically restricted by the solid material's structure, resulting in lower ionic or electronic conductivity compared to liquid electrolytes. However, the presence of percolation channels can significantly enhance the conductivity of solid electrolytes by providing pathwaysfor the rapid movement of ions or electrons.There are several mechanisms that can lead to the formation of solid electrolyte percolation channels. One such mechanism is structural defects within the solid electrolyte. These defects, such as vacancies or grain boundaries, can act as channels for ion or electron movement. Another mechanism involves the formation of special structures during the preparation of solid electrolytes. For instance, nanoparticles or nanowires can create percolation channels that facilitate ion or electron transport.Additionally, the addition of specific additives to solid electrolytes can promote the formation anddistribution of percolation channels. These additives, such as conductive agents or modifiers, can enhance the conductivity of the solid electrolyte by creating a network of conductive pathways.The properties and formation of solid electrolyte percolation channels are influenced by various factors. Onesuch factor is the material composition of the solid electrolyte, as different materials may exhibit different percolation behaviors. The microstructure of the solid electrolyte, including its grain size, porosity, and defect structure, also plays a crucial role in percolation channel formation.Moreover, the operating conditions of the electrochemical device, such as temperature and pressure, can affect the percolation properties of the solid electrolyte. For instance, changes in temperature can alter the ionic mobility and diffusion kinetics within the solid electrolyte, affecting the efficiency of percolation channels.The study of solid electrolyte percolation is crucial for understanding and improving the performance of electrochemical devices. By understanding the mechanisms and influencing factors of solid electrolyte percolation, researchers can design better solid electrolytes with improved ionic or electronic conductivity, leading to more efficient and durable electrochemical devices.In conclusion, solid electrolyte percolation is a critical process that enables efficient ion or electron transport within solid electrolytes. The formation of percolation channels, influenced by factors such as material composition, microstructure, and operating conditions, plays a pivotal role in determining the conductivity and performance of solid electrolytes.Ongoing research in this field aims to further understand and optimize solid electrolyte percolation for improved electrochemical device performance.。

氟醚橡胶在不同介质下的热老化行为与机理研究

氟醚橡胶在不同介质下的热老化行为与机理研究

装备环境工程第20卷第12期·70·EQUIPMENT ENVIRONMENTAL ENGINEERING2023年12月氟醚橡胶在不同介质下的热老化行为与机理研究刘俊邦1,张少锋1,李璞2,张洪彬1,陈荻云1,唐庆云1*(1.工业和信息化部电子第五研究所,广州 510610;2.中国航发湖南动力机械研究所,湖南 株洲 412000)摘要:目的对氟醚橡胶FM-2D在空气与飞马Ⅱ号润滑油中的热老化行为与机理进行研究。

方法开展氟醚橡胶高温贮存试验,在热氧、热油的介质环境下,研究氟醚橡胶的力学性能退化规律。

试验后对样品的拉伸性能、压缩性能以及硬度进行检测,并且利用傅里叶红外光谱仪、扫描电子显微镜以及X射线电子能谱对试验后样品进行检测。

结果通过热老化试验,发现氟醚橡胶在200 ℃以下能够长期维持较好的力学性能。

试验温度在200 ℃以上,氟醚橡胶的力学性能出现明显退化趋势,并且在热空气与热油中的老化趋势不同。

在220 ℃的热空气老化31 d后,氟醚橡胶的拉伸强度下降27.0%,断裂伸长率增大89.8%,压缩应力松弛率为34.6%,硬度下降8.7%。

在220 ℃的热油老化31 d后,氟醚橡胶的拉伸强度下降85.9%,断裂伸长率下降83.9%,压缩应力松弛率为‒17.5%,硬度上升4.2%。

结论在热空气老化过程中,橡胶分子链受热氧影响发生断裂,使其强度下降;在热油老化过程中,油介质和高温的耦合作用使橡胶的交联网络失效,橡胶发硬变脆。

关键词:氟醚橡胶;热老化;力学性能;X射线光电子能谱中图分类号:TN06 文献标识码:A 文章编号:1672-9242(2023)12-0070-08DOI:10.7643/ issn.1672-9242.2023.12.009Thermal Aging Behavior and Mechanism of Fluoroether Rubber under Different Media LIU Jun-bang1, ZHANG Shao-feng1, LI Pu2, ZHANG Hong-bin1, CHEN Di-yun1, TANG Qing-yun1*(1. Electronic Fifth Institute of the Ministry of Industry and Information Technology, Guangzhou 510610, China;2. China Aerospace Hunan Power Machinery Research Institute, Hunan Zhuzhou 412000, China)ABSTRACT: The work aims to study the thermal aging behavior and mechanism of fluoroether rubber FM-2D in air and Pegasus II lubricating oil. The storage test of fluoroether rubber at high temperature was carried out, and the degradation law of mechanical properties of fluoroether rubber was investigated in air and oil. The tensile properties, compressive properties and hardness of the samples were tested after the aging test. A Fourier infrared spectrometer, a scanning electron microscope and an X-ray electron spectroscopy were used to detect and analyze the samples after the test to explore the aging mechanism. The re-sult showed that fluoroether rubber could maintain good mechanical properties for a long time at 200 ℃. While when the tem-perature was above 200 ℃, the mechanical properties of fluoroether rubber degraded obviously. After 31 days of aging in hot air收稿日期:2023-10-31;修订日期:2023-12-11Received:2023-10-31;Revised:2023-12-11引文格式:刘俊邦, 张少锋, 李璞, 等. 氟醚橡胶在不同介质下的热老化行为与机理研究[J]. 装备环境工程, 2023, 20(12): 70-77.LIU Jun-bang, ZHANG Shao-feng, LI Pu, et al. Thermal Aging Behavior and Mechanism of Fluoroether Rubber under Different Media[J]. Equipment Environmental Engineering, 2023, 20(12): 70-77.第20卷第12期刘俊邦,等:氟醚橡胶在不同介质下的热老化行为与机理研究·71·at 220 ℃, the tensile strength of fluoroether rubber decreased by 27.0%, the elongation at break increased by 89.8%, the relaxa-tion rate of compressive stress was 34.6%, and the hardness decreased by 8.7%. After 31 days of hot oil aging at 220 ℃, the tensile strength of fluoroether rubber decreased by 85.9%, the elongation at break decreased by 83.9%, the relaxation rate of compressive stress was ‒17.5%, and the hardness increased by 4.2%. Through analysis and characterization, it is founded that the molecular chain of rubber is broken under the influence of hot oxygen during the aging process of hot air, and the strength of rubber decreases. In hot oil aging, the coupling effect of oil medium and high temperature makes the crosslinking network of rubber fail, and the rubber becomes hard and brittle.KEY WORDS: fluoroether rubber; FM-2D; thermal aging; mechanical properties; X-ray photoelectron spectroscopy橡胶以O形圈、垫片的形式被应用于液体和气体的密封,广泛应用在机械、化工、航空航天、汽车等领域[1-4]。

河南工业大学土木工程专业作业英语作业

河南工业大学土木工程专业作业英语作业

Unit10:水密性浸入隧道虽然水密性是任何沉管的隧道设计的首要目标之一,设计不会亏如果(附带太小被忽略)。

隧道元素的大型外围表面上未检测到的建设缺失的混凝土或防水膜或钢焊缝中未检测到针孔的可能性不能完全为直纹的。

适当的维修方法存在和设计中,必须指定。

水压力与隧道墙系统中必须避免的。

提供适当的排水入内排水系统。

此渗漏很小,不需要额外的排水和水仓容量。

对于钢壳隧道元素,是纯粹由钢外壳本身提供的。

水密性依赖于大量的焊缝的质量。

内壳的混凝土是在压缩下的横向。

对于混凝土隧道,泄漏有关的防水膜的质量,如果使用的话,和裂缝的发展。

因此,在横向和纵向方向上的不同的结构的行为的理解是很重要的。

在横向方向上,盒形的钢筋混凝土隧道总是有经历弯曲张力在屋顶和底板的区域,即使在横向压缩。

的隧道段被设计成使得所得到的破解可以仅部分地渗透在压缩区足够厚,以避免通过缝隙泄漏,离开混凝土。

在纵向的方向,强调是多低幅度比横向方向。

基本压力是压缩。

二级影响,可能会导致局部紧张不应导致全面深度裂缝。

热收缩裂缝是典型的辅助效果。

在厚厚的混凝土构件,水化热导致大量加热的成员。

一段时间后该成员将冷却到环境温度。

稀土盛鸿现在硬化混凝土的收缩可能会受到限制。

为了保证充足,这发生在铸造到在较早阶段铸造的底板上墙。

连接到刚性底板墙的冷却收缩的结果是磁珠在底板和墙的底部部分中的纵向拉伸应变。

除非采取适当的措施,因此垂直深度的全方位的裂缝可以发生在约5米的间隔。

制定了令人满意的进程,以避免这些施工裂缝,即通过减少水化,热和使用具有相对较低的水泥含量和强迫冷却的墙壁的下半部分的混凝土。

有时这样做是与绝缘和基地合板加热相结合。

如果不过发现裂缝,补救灌浆似乎有效。

微分热发展的有效控制很大程度上取决于混凝土的热量。

这一进程,反过来,是量的行政长官发挥了其中的直接职能。

因此,典型混凝土混与高水泥因素(摘自公路结构)的使用可以在这方面的。

有关于控制混凝土隧道渗漏的两个基本概念:扩大联合概念混凝土隧道防水的扩张联合概念涉及通过避免跨韵文实现水密性混凝土的开裂。

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In this article, we propose an explanation for the experimental results which is based on two key observations. First, at filling factors ν < 1, strong and subtle correlations exist in the bulk of a 2D electron gas, even when it is compressible. Tunneling at low energies is extremely strongly suppressed because states with an uncorrelated electron inserted or removed are nearly orthogonal to the low-energy states in which all electrons are strongly correlated.16 This property is established by bulk 2D-2D tunneling experiments17 which manifest a wide gap in the TDOS at all values of ν. Like their edge counterparts, bulk-TDOS results exhibit surprisingly little dependence on the occurrence or absence of the quantum Hall effect. Second, in any finite quantum-Hall system, there exists a series of low-energy excitations which are generated by electronically rigid deformations of the system periphery. We will refer to these as periphery-deformation (PD) excitations. We propose that in systems where the confining potential is smooth enough that electrons remain strongly correlated at the edge, tunneling electrons can be accommodated, at low energies, only by periphery deformations. In the following, we explain why PD excitations are generic, and establish the properties underlying the edge-TDOS observations.
(February 1, 2008)
arXiv:cond-mat/9802019v2 [cond-mat.mes-hall] 14 Apr 1999பைடு நூலகம்
We argue that, at any filling factor ν, correlated quantum-Hall systems possess a set of chiral boson excitations which are generated by electronically rigid deformations of the system’s periphery. We submit that tunneling electrons can be accommodated, at low energies, in these systems only by periphery-deformation excitations. This property would explain the recent observation of a tunneling density of states at the edge which does not exhibit a strong dependence on the occurrence or absence of the quantum Hall effect and has a power-law dependence on energy with exponent ν−1 − 1.
energy gap for particle-hole excitations in the bulk and low-lying excitations are localized at the boundary of the finite 2D electron system.4 The edge electrons then constitute a particularly intriguing realization of a onedimensional (1D) electron system.5 In the simplest case, they are described by a chiral-Luttinger-liquid (χLL)6
fine tuning of parameters in order to be consistent with generalized χLL and other models11,12 which have been proposed for edges at ν = 1/m. Most surprising, the power-law behavior was found to be insensitive to the occurrence or absence of the quantum Hall effect, even though the very use of a 1D model for the microscopic electron physics springs from the excitation gap in the bulk of the 2D system. The simple single-branch χLL model appears to apply in circumstances where it had seemed clear that it could not apply. These important experiments have spurred intense theoretical effort12–15 aimed at resolving this puzzle and identifying the character of the revision apparently required of FQH edgephysics theory.
PACS number(s): 73.40.Gk, 73.40.Hm
Experimental and theoretical studies of twodimensional (2D) electron systems in strong perpen-
dicular magnetic fields have uncovered a rich body of many-particle physics.1 For magnetic fields sufficiently
of chiral 1D excitations present. The present work is motivated by recent experimental
studies of tunneling into fractional-quantum-Hall (FQH) edges. At filling factor ν = 1/3, the low-energy TDOS was found9 to vary approximately as
model which contains only the right-moving degrees of freedom of a conventional 1D electron system. The chiral attribute is permitted because the magnetic field breaks time-reversal symmetry. The χLL model predicts that the electronic tunneling density of states (TDOS)
strong and densities sufficiently low, electrons occupy only states in the lowest Landau level (LLL) which have identical kinetic energies.2 In this zero-band-width correlation problem, interactions alone control the low-
A>(ε)

ε1 ν
−1
,
(1)
in agreement with predictions based on χLL theory. However, subsequent experiments10 found that the
TDOS is described by Eq. (1) equally well over the entire range 1/4 ≤ ν ≤ 1. This experimental result requires
at fractional filling factors vanishes as a power law at small energies. The simple χLL model is expected to apply only for ν = 1/m with m odd and, even then, only when the 2D electron system has a sharp edge. More generally,7,8 the edge system is expected to be described by generalized 1D electron models with several branches
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